globalchange  > 气候变化与战略
DOI: 10.1016/j.tecto.2021.228917
论文题名:
Stretching in continental back-arc basins: Insights from subsidence analysis of the Neuquén Basin, Argentina
作者: Scivetti N.; Marcos P.; Pivetta C.P.; Benedini L.; Falco J.I.; Arrouy M.J.; Bahía M.E.; Franzese J.R.; Gregori D.A.
刊名: Tectonophysics
ISSN: 00401951
出版年: 2021
卷: 812
语种: 英语
中文关键词: Crustal and lithospheric thickness ; Neuquén Basin ; Stretching factor ; Subsidence analysis
英文关键词: Geodesy ; Subsidence ; Tectonics ; Back-arc basin ; Elastic thickness ; Forward modelling ; Forward models ; Initial thickness ; Lithosphere structure ; Lithospheric ; Lithospheric structure ; Structural geology ; backarc basin ; continental arc ; crustal thickness ; lithospheric structure ; outcrop ; subsidence ; tectonics ; Argentina ; Neuquen Basin
英文摘要: In the present contribution, we apply forward modelling and subsidence analysis to determine the initial lithospheric structure and the Neuquén Basin central area's stretching factor. The forward models determined that the initial thickness of the crust and the lithosphere would have been around 30 km and 100 km, respectively. Airy and regional isostasy models were considered for the calculation of the tectonic subsidence in outcrops and the subsurface. In both cases, results are very similar due to an elastic thickness of ~3 km for the beginning of the basin, which allows considering the Airy isostasy model as the representative for the analyzed period in the study area. Regarding the stretching factor, the results suggest that the extension varies between 1 and 1.32 for the analyzed area. Although these values seem to be higher than the previous estimations for the Neuquén Basin, they are consistent with those mentioned in the literature for the back-arc basins around the world with similar lithosphere structure and tectonic subsidence values. Furthermore, it should be mentioned that similar tectonic subsidence values could be obtained for the same area considering a lower stretching factor and a westward lithospheric thickening associated with the Neopaleozoic orogeny. © 2021 Elsevier B.V.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/170900
Appears in Collections:气候变化与战略

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作者单位: Instituto Geológico del Sur (INGEOSUR), Universidad Nacional del Sur (UNS)-CONICET, Bahía Blanca, Argentina; Departamento de Geología, Universidad Nacional del Sur (UNS), Bahía Blanca, Argentina; Universidad Nacional de Río Negro, Instituto de Investigación en Paleobiología y Geología, Av. Roca 1242, General Roca, Río Negro R8332EXZ, Argentina; IIPG, UNRN, CONICET, General Roca, Argentina; Instituto de Investigaciones en Diversidad Cultural y Procesos de Cambio (IIDyPCa), CONICET - Universidad Nacional de Río Negro, Mitre 630, San Carlos de Bariloche, CP 8400, Argentina; Instituto de Hidrología de Llanuras “Dr. Eduardo Jorge Usunoff” (IHLLA), CIC - CONICET – UNICEN, Argentina; Departamento de Física, Universidad Nacional del Sur (UNS), Bahía Blanca; Centro de Investigaciones Geológicas (CIG), Universidad Nacional de La Plata (UNLP)-CONICET, Diag. 113 n° 275, La Plata, 1900, Argentina

Recommended Citation:
Scivetti N.,Marcos P.,Pivetta C.P.,et al. Stretching in continental back-arc basins: Insights from subsidence analysis of the Neuquén Basin, Argentina[J]. Tectonophysics,2021-01-01,812
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